Situated in the
Demanovska valley northerly to the Demanovska Cave of
Liberty, in the National Nature Reserve Demanovska
Valley, in the territory of the Low Tatras National
Park. The cave was created in the Middle Triassic
limestones by the former ponor flow of Demanovka, at
three developmental levels. It is 1,975 m long. Ice
filling occurs in the lower parts of the cave. Ground
ice, ice columns, stalactites and stalagmites are
present. A finding place of bones of various vertebrates
including speleal bear (Ursus spelaeus), that
were erroneously taken for dragon bones in the 18th
century. The cave has been known since the time
immemorial. The cave was surveyed by G. Buchholtz Jr in
1719-1723. Numerous inscriptions on its walls and a lot
of preserved rich literary resources evidence a great
interest about this cave. The cave was open to the
public in the eighties of the last century, and reopen
in 1950-1952. Currently, publicly accessible are 650 m.
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